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Some glacial deposition features include moraines, drumlins, eskers, and outwash plains. These features are a result of the deposition of sediment and rocks carried by glaciers as they move and melt.
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Some features formed by glacial deposition include moraines (ridges of till), drumlins (elongated hills), eskers (sinuous ridges of sand and gravel), and kettles (depressions formed by melting ice blocks).
Mosses and ferns are typically considered pioneer species because they are some of the first plants to colonize an area during primary succession. They help to build up soil and provide habitat for other species to establish and develop.
Some deposits of alpine glaciers include moraines (such as lateral, medial, and terminal moraines), drumlins, eskers, and outwash plains. These deposits are created as the glacier erodes, transports, and deposits sediment during its movement.
Some examples of pioneer species include mosses, lichens, and certain grasses. These species are the first to colonize barren or disturbed areas, helping to establish soil and create habitat for other plant species to follow.
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Erratics are a key sign of glacial activity. These are large rocks resting on top of soil, unlike monadnocks which are pinnacles left over from riparian erosion. The rock is carried from some distant mountain on glacial ice, and abandoned on a plain when the ice stops moving and melts. Glacial valleys have a characteristic U shape to them, as opposed to the V shape of valleys carved by water. Often glaciers leave broken rock and rubble in a wavey line known as a terminal moraine, or along the sides of the moving ice in formations known as lateral moraines. Ice also gouges series of characteristic grooves or scars on mountain rock faces, indicative of glacial activity.
After the eruption, plants began to colonize the volcanic debris. Such plants that is called pioneer species
Some famous moraines in the US include the terminal moraine of the Wisconsin glaciation in Long Island, New York, and the moraines left behind by the glaciers in Glacier National Park in Montana and Denali National Park in Alaska.
Some of moraines types are rogen and veiki Moraines,Generally moraines can be classified either by their origin, location with respect to a glacier or former glacier, or by their shape.The first approach is suitable for moraines associated to contemporary glaciers but more difficult to apply to old moraines whose glaciers have disappeared long ago.Moraines types like rogen and veiki moraines are defined by their particular morphology since their origin has been a matter of dispute. Some moraine types are only known from ancient glaciers, like the two former ones, while medial moraines of valley glaciers are poorly preserved and difficult to distinguish after the retreat or melting of the glacier.Refer to link below for more details.
Common sediments produced by glaciers include till (unsorted mixture of rocks and sediment), moraine (deposits of till), outwash (sorted sediments deposited by meltwater), and glacial erratics (large boulders transported by glaciers from distant locations).